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Conference Paper: Angular characteristics of the Pathfinder AVHRR land thermal data and radiative transfer modeling

TitleAngular characteristics of the Pathfinder AVHRR land thermal data and radiative transfer modeling
Authors
Issue Date1994
Citation
International Geoscience and Remote Sensing Symposium (IGARSS), 1994, v. 1, p. 61-63 How to Cite?
AbstractIn order to understand the angular characteristics observed from the Pathfinder AVHRR land thermal data, a simplified narrow-band radiative transfer model is developed based on a series of approximations for the vertical structures of the atmospheric conditions, which also take into account the directional variation of the upwelling surface radiation. The LOWTRAN-7 code is then applied to validate the present model. Different water vapor content, air temperature and surface temperature are used to simulate the AVHRR ch4/ch5 radiance at the top of the atmosphere as the function of the viewing zenith angle. A directional snow emissivity model and measured emissivity of the agricultural soil are inputed into this model to evaluate the effects of the surface anisotropity on the AVHRR ch4/ch5 radiance. Upwelling radiance usually decreases as the viewing zenith angle increases in thermal regions. However, the angular pattern may reverse when the air temperature is larger than surface temperature.
Persistent Identifierhttp://hdl.handle.net/10722/321222

 

DC FieldValueLanguage
dc.contributor.authorLiang, Shunlin-
dc.contributor.authorRanson, K. Jon-
dc.date.accessioned2022-11-03T02:17:28Z-
dc.date.available2022-11-03T02:17:28Z-
dc.date.issued1994-
dc.identifier.citationInternational Geoscience and Remote Sensing Symposium (IGARSS), 1994, v. 1, p. 61-63-
dc.identifier.urihttp://hdl.handle.net/10722/321222-
dc.description.abstractIn order to understand the angular characteristics observed from the Pathfinder AVHRR land thermal data, a simplified narrow-band radiative transfer model is developed based on a series of approximations for the vertical structures of the atmospheric conditions, which also take into account the directional variation of the upwelling surface radiation. The LOWTRAN-7 code is then applied to validate the present model. Different water vapor content, air temperature and surface temperature are used to simulate the AVHRR ch4/ch5 radiance at the top of the atmosphere as the function of the viewing zenith angle. A directional snow emissivity model and measured emissivity of the agricultural soil are inputed into this model to evaluate the effects of the surface anisotropity on the AVHRR ch4/ch5 radiance. Upwelling radiance usually decreases as the viewing zenith angle increases in thermal regions. However, the angular pattern may reverse when the air temperature is larger than surface temperature.-
dc.languageeng-
dc.relation.ispartofInternational Geoscience and Remote Sensing Symposium (IGARSS)-
dc.titleAngular characteristics of the Pathfinder AVHRR land thermal data and radiative transfer modeling-
dc.typeConference_Paper-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1109/IGARSS.1994.399022-
dc.identifier.scopuseid_2-s2.0-0028734190-
dc.identifier.volume1-
dc.identifier.spage61-
dc.identifier.epage63-

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